Helium and methane sources and fluxes of shallow submarine hydrothermal plumes near the Tokara Islands, Southern Japan

Hsin Yi Wen, Yuji Sano, Naoto Takahata, Yama Tomonaga, Akizumi Ishida, Kentaro Tanaka, Takanori Kagoshima, Kotaro Shirai, Jun Ichiro Ishibashi, Hisayoshi Yokose, Urumu Tsunogai, Tsanyao F. Yang

研究成果: ジャーナルへの寄稿記事

6 引用 (Scopus)

抄録

Shallow submarine volcanoes have been newly discovered near the Tokara Islands, which are situated at the volcanic front of the northern Ryukyu Arc in southern Japan. Here, we report for the first time the volatile geochemistry of shallow hydrothermal plumes, which were sampled using a CTD-RMS system after analyzing water column images collected by multi-beam echo sounder surveys. These surveys were performed during the research cruise KS-14-10 of the R/V Shinsei Maru in a region stretching from the Wakamiko Crater to the Tokara Islands. The 3 He flux and methane flux in the investigated area are estimated to be (0.99-2.6) × 10 4 atoms/cm 2/sec and 6-60 t/yr, respectively. The methane in the region of the Tokara Islands is a mix between abiotic methane similar to that found in the East Pacific Rise and thermogenic one. Methane at the Wakamiko Crater is of abiotic origin but affected by isotopic fractionation through rapid microbial oxidation. The helium isotopes suggest the presence of subduction-type mantle helium at the Wakamiko Crater, while a larger crustal component is found close to the Tokara Islands. This suggests that the Tokara Islands submarine volcanoes are a key feature of the transition zone between the volcanic front and the spreading back-arc basin.

元の言語英語
記事番号34126
ジャーナルScientific reports
6
DOI
出版物ステータス出版済み - 9 27 2016

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hydrothermal plume
helium
methane
submarine volcano
crater
helium isotope
echo sounder
isotopic fractionation
transition zone
subduction
water column
geochemistry
mantle
oxidation
basin

All Science Journal Classification (ASJC) codes

  • General

これを引用

Wen, H. Y., Sano, Y., Takahata, N., Tomonaga, Y., Ishida, A., Tanaka, K., ... Yang, T. F. (2016). Helium and methane sources and fluxes of shallow submarine hydrothermal plumes near the Tokara Islands, Southern Japan. Scientific reports, 6, [34126]. https://doi.org/10.1038/srep34126

Helium and methane sources and fluxes of shallow submarine hydrothermal plumes near the Tokara Islands, Southern Japan. / Wen, Hsin Yi; Sano, Yuji; Takahata, Naoto; Tomonaga, Yama; Ishida, Akizumi; Tanaka, Kentaro; Kagoshima, Takanori; Shirai, Kotaro; Ishibashi, Jun Ichiro; Yokose, Hisayoshi; Tsunogai, Urumu; Yang, Tsanyao F.

:: Scientific reports, 巻 6, 34126, 27.09.2016.

研究成果: ジャーナルへの寄稿記事

Wen, HY, Sano, Y, Takahata, N, Tomonaga, Y, Ishida, A, Tanaka, K, Kagoshima, T, Shirai, K, Ishibashi, JI, Yokose, H, Tsunogai, U & Yang, TF 2016, 'Helium and methane sources and fluxes of shallow submarine hydrothermal plumes near the Tokara Islands, Southern Japan', Scientific reports, 巻. 6, 34126. https://doi.org/10.1038/srep34126
Wen, Hsin Yi ; Sano, Yuji ; Takahata, Naoto ; Tomonaga, Yama ; Ishida, Akizumi ; Tanaka, Kentaro ; Kagoshima, Takanori ; Shirai, Kotaro ; Ishibashi, Jun Ichiro ; Yokose, Hisayoshi ; Tsunogai, Urumu ; Yang, Tsanyao F. / Helium and methane sources and fluxes of shallow submarine hydrothermal plumes near the Tokara Islands, Southern Japan. :: Scientific reports. 2016 ; 巻 6.
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abstract = "Shallow submarine volcanoes have been newly discovered near the Tokara Islands, which are situated at the volcanic front of the northern Ryukyu Arc in southern Japan. Here, we report for the first time the volatile geochemistry of shallow hydrothermal plumes, which were sampled using a CTD-RMS system after analyzing water column images collected by multi-beam echo sounder surveys. These surveys were performed during the research cruise KS-14-10 of the R/V Shinsei Maru in a region stretching from the Wakamiko Crater to the Tokara Islands. The 3 He flux and methane flux in the investigated area are estimated to be (0.99-2.6) × 10 4 atoms/cm 2/sec and 6-60 t/yr, respectively. The methane in the region of the Tokara Islands is a mix between abiotic methane similar to that found in the East Pacific Rise and thermogenic one. Methane at the Wakamiko Crater is of abiotic origin but affected by isotopic fractionation through rapid microbial oxidation. The helium isotopes suggest the presence of subduction-type mantle helium at the Wakamiko Crater, while a larger crustal component is found close to the Tokara Islands. This suggests that the Tokara Islands submarine volcanoes are a key feature of the transition zone between the volcanic front and the spreading back-arc basin.",
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